
木栓質(zhì),木栓質(zhì)體,木栓質(zhì)煤素質(zhì)
The results of fluorescence evalution of cutinite and suberinite show th... 煤中角質(zhì)體和木栓質(zhì)體的光性演化表明其對本區(qū)煤成油有一定的貢獻。
Suberinite occurs commonly in Mesozoic coal measures and terrestrial organic matter source rocks in Northwest China, which is formed from suberized cell walls, particularly in plant periderm. 西北中生界煤系烴源巖中普遍含有木栓質(zhì)體,它來源于植物周皮的木栓化細胞壁。
Keywords Peat;Suberinite;Oxidation;Decomposition;Fluorescence; 泥炭;木栓質(zhì)體;氧化;分解;熒光;
Keywords suberinite;hydrocarbon generating evolution;thermal simulation experiment; 木栓質(zhì)體成烴演化熱;模擬實驗;
Keywords Coal measures;Oil source rock;Coal composition;Mesozoic era;Suberinite; 煤系;生油層;中生代;煤組分;木栓質(zhì)體;